It is found that the degree of mineralization and metamorphic coefficient and conversion potential of formation water , the fault is zone of sluicing of atmospheric infiltration water flowing from basin west margin to east ( centripetal flow ) and sedimentary compaction water flowing from qija gulong depression to west ( centrifugal flow ) 通過地層水礦化度和變質(zhì)系數(shù)等參數(shù)的分布規(guī)律及一系列折算水位剖面圖的分析發(fā)現(xiàn),該斷裂對水是不封閉的,并且是盆地西緣大氣滲入水向東流動(向心流)及齊家古龍坳陷沉積壓實水向西流動(離心流)的共同泄水帶。